FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2945260015> ?p ?o ?g. }

• W2945260015 endingPage "115" @default.
• W2945260015 startingPage "103" @default.
• W2945260015 abstract "Abstract Soil organic matter (SOM) is sensitive to land use and to physico-chemical soil properties as well soil microbial communities controlling SOM stabilization. Our study aimed at exploring how carbonates of Mediterranean soils – known to stabilize SOM by enhancing soil aggregation and binding SOM by calcium – are affecting SOM and microbial communities under different land uses. In soils with and without carbonates sampled in forests, cultivated and abandoned fields, we have fractionated SOM-pools according to particle sizes and determined C mineralization rates and polyvalent cations in these fractions. In agreement with larger scale assessments in the Mediterranean, our results show that SOM contents are greater in forest than in agricultural soils, but that the differences among land use types depend on carbonate contents. While SOM contents are greater in carbonated soils of forests, cultivated soils have low SOM levels independent of the carbonate content, presumably due to a reduced protection of particulate SOM by century-long intense tillage. Forest soils contain particularly large amounts of SOM associated with the coarser soil fraction. In this fraction, C mineralization was smallest in the carbonated forest soil, possibly due to a low SOM quality indicated by high C/N ratios and low δ15N values. Greater contents of Ca, Fe and Al in carbonated soils also suggests that stabilization through Ca and phyllosilicates was important. Mineralization of sand-associated SOM was highest in cultivated and abandoned soils, which is indicative for a small SOM stabilization, which in turn might restrict SOM accumulation after land abandonment. Microbial communities assessed by phospho-lipid fatty acid signatures and microbial carbon use efficiency were more closely associated with land use than with carbonate content – a pattern that reflects the distribution of C pools among size fractions which differed more strongly among land use types than between soils with and without carbonates." @default.
• W2945260015 created "2019-05-29" @default.
• W2945260015 creator A5017721581 @default.
• W2945260015 creator A5037977390 @default.
• W2945260015 creator A5060814818 @default.
• W2945260015 creator A5089042170 @default.
• W2945260015 date "2019-10-01" @default.
• W2945260015 modified "2023-10-10" @default.
• W2945260015 title "Effect of land use and carbonates on organic matter stabilization and microbial communities in Mediterranean soils" @default.
• W2945260015 cites W1599552059 @default.
• W2945260015 cites W1685833191 @default.
• W2945260015 cites W1980680725 @default.
• W2945260015 cites W1985777199 @default.
• W2945260015 cites W1987864646 @default.
• W2945260015 cites W1988672594 @default.
• W2945260015 cites W1993010269 @default.
• W2945260015 cites W1994844048 @default.
• W2945260015 cites W2005155021 @default.
• W2945260015 cites W2013661555 @default.
• W2945260015 cites W2013927755 @default.
• W2945260015 cites W2031683967 @default.
• W2945260015 cites W2040442433 @default.
• W2945260015 cites W2043394795 @default.
• W2945260015 cites W2045641952 @default.
• W2945260015 cites W2052425114 @default.
• W2945260015 cites W2054838452 @default.
• W2945260015 cites W2056086102 @default.
• W2945260015 cites W2065159933 @default.
• W2945260015 cites W2065781824 @default.
• W2945260015 cites W2067439971 @default.
• W2945260015 cites W2072145396 @default.
• W2945260015 cites W2077514410 @default.
• W2945260015 cites W2080666601 @default.
• W2945260015 cites W2082379988 @default.
• W2945260015 cites W2087982985 @default.
• W2945260015 cites W2090297484 @default.
• W2945260015 cites W2091460828 @default.
• W2945260015 cites W2095589143 @default.
• W2945260015 cites W2112520156 @default.
• W2945260015 cites W2116598828 @default.
• W2945260015 cites W2117321971 @default.
• W2945260015 cites W2120730459 @default.
• W2945260015 cites W2123129893 @default.
• W2945260015 cites W2132484323 @default.
• W2945260015 cites W2134539878 @default.
• W2945260015 cites W2139111904 @default.
• W2945260015 cites W2139405554 @default.
• W2945260015 cites W2143363222 @default.
• W2945260015 cites W2145821233 @default.
• W2945260015 cites W2161436803 @default.
• W2945260015 cites W2163103579 @default.
• W2945260015 cites W2163538224 @default.
• W2945260015 cites W2166135450 @default.
• W2945260015 cites W2178655169 @default.
• W2945260015 cites W2200817828 @default.
• W2945260015 cites W2300552860 @default.
• W2945260015 cites W2474622149 @default.
• W2945260015 cites W2525110493 @default.
• W2945260015 cites W2587555969 @default.
• W2945260015 cites W2600465625 @default.
• W2945260015 cites W270066167 @default.
• W2945260015 cites W2910689128 @default.
• W2945260015 cites W4241980718 @default.
• W2945260015 cites W4245570257 @default.
• W2945260015 doi "https://doi.org/10.1016/j.geoderma.2019.05.021" @default.
• W2945260015 hasPublicationYear "2019" @default.
• W2945260015 type Work @default.
• W2945260015 sameAs 2945260015 @default.
• W2945260015 citedByCount "30" @default.
• W2945260015 countsByYear W29452600152019 @default.
• W2945260015 countsByYear W29452600152020 @default.
• W2945260015 countsByYear W29452600152021 @default.
• W2945260015 countsByYear W29452600152022 @default.
• W2945260015 countsByYear W29452600152023 @default.
• W2945260015 crossrefType "journal-article" @default.
• W2945260015 hasAuthorship W2945260015A5017721581 @default.
• W2945260015 hasAuthorship W2945260015A5037977390 @default.
• W2945260015 hasAuthorship W2945260015A5060814818 @default.
• W2945260015 hasAuthorship W2945260015A5089042170 @default.
• W2945260015 hasConcept C107872376 @default.
• W2945260015 hasConcept C159390177 @default.
• W2945260015 hasConcept C159750122 @default.
• W2945260015 hasConcept C182124840 @default.
• W2945260015 hasConcept C185592680 @default.
• W2945260015 hasConcept C18903297 @default.
• W2945260015 hasConcept C39432304 @default.
• W2945260015 hasConcept C4646841 @default.
• W2945260015 hasConcept C4792198 @default.
• W2945260015 hasConcept C48743137 @default.
• W2945260015 hasConcept C86803240 @default.
• W2945260015 hasConceptScore W2945260015C107872376 @default.
• W2945260015 hasConceptScore W2945260015C159390177 @default.
• W2945260015 hasConceptScore W2945260015C159750122 @default.
• W2945260015 hasConceptScore W2945260015C182124840 @default.
• W2945260015 hasConceptScore W2945260015C185592680 @default.
• W2945260015 hasConceptScore W2945260015C18903297 @default.
• W2945260015 hasConceptScore W2945260015C39432304 @default.
• W2945260015 hasConceptScore W2945260015C4646841 @default.

• next